The Lusatian Fault (German: Lausitzer Verwerfung), formerly Lusatian Overthrust (Lausitzer Überschiebung), is the most important geological disturbance...

This list covers all faults and fault-systems that are either geologically important[clarification needed] or connected to prominent seismic activity.[clarification...

northern ridge is marked by the Lusatian Fault, a geological disturbance zone separating the Bohemian sandstones from the Lusatian granodiorite. During the Tertiary...

deepest incision. Later the Lusatian granodiorite was uplifted over the 600 metre thick sandstone slab along the Lusatian Fault and pushed it downwards until...

The West Lusatian Hill Country and Uplands (German: Westlausitzer Hügel- und Bergland), sometimes just the West Lusatian Hills, is a natural region in...

Mountains Kaczawskie Foothills Lusatian Mountains Lusatian Highlands Lusatian Gefilde West Lusatian Foothills East Lusatian Foothills Rudawy Janowickie Jelenia...

Polenz The Polenz valley immediately above the Lusatian Fault Location Country Germany State Saxony Physical characteristics Source    • location in Saxony...

typically accompanied with trilling of the uvula [ʀ̝̊], so that brach /ˈbrax/ 'fault' is typically pronounced [bʁaʀ̝̊]. /x/ does not occur word-initially, whereas...

smooth polished, petrified rock. The cause was tectonic movements of the Lusatian Fault, about 900 metres away; here during the Cretaceous era, the older granite...

the upland is bordered by the Dresden Elbe valley, running along the Lusatian fault, where the elevation steeply falls 200 metres to the Dresden Elbe valley...